All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Long-Term Trends in the Upper Atmosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F21%3A00543128" target="_blank" >RIV/68378289:_____/21:00543128 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1002/9781119815631.ch17" target="_blank" >http://dx.doi.org/10.1002/9781119815631.ch17</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/9781119815631.ch17" target="_blank" >10.1002/9781119815631.ch17</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Long-Term Trends in the Upper Atmosphere

  • Original language description

    The increasing concentration of greenhouse gases, particularly of CO2, affects the upper atmosphere (mesosphere, thermosphere, and ionosphere) remarkably stronger than the troposphere and surface. However, the effect in the upper atmosphere is greenhouse cooling, not warming. It has more or less impact on all parameters in the upper atmosphere (neutral, ion and electron temperatures and densities, winds etc.), which is summarized in the qualitatively consistent scenario of global change in the upper atmosphere. Main compounds of this scenario are long-term trends in temperature and electron density at various heights but it also includes trends in some other parameters like the thermospheric neutral density. On the other hand, there are still significant gaps in the trend scenario, particularly trends in winds and atmospheric wave activity. These gaps and discrepancies will be the topic of investigations in the near future. The greenhouse gases are the main driver of long-term trends in the upper atmosphere but some role is played also by other drivers like ozone or the secular change of the Earth's magnetic field. These other trend drivers are responsible for the trends in the upper atmosphere to vary temporally and spatially to some extent.

  • Czech name

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

  • OECD FORD branch

    10509 - Meteorology and atmospheric sciences

Result continuities

  • Project

    <a href="/en/project/GA18-01625S" target="_blank" >GA18-01625S: The influence of greenhouse gases and other drivers on long-term trends in the stratosphere-mesosphere-thermosphere-ionosphere system</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Book/collection name

    Upper Atmosphere Dynamics and Energetics

  • ISBN

    978-1-119-50756-7

  • Number of pages of the result

    17

  • Pages from-to

    325-341

  • Number of pages of the book

    560

  • Publisher name

    American Geophysical Union

  • Place of publication

    Hoboken

  • UT code for WoS chapter

    000877517900018